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Andrew J. Watson
Researcher at University of Exeter
Publications - 531
Citations - 38911
Andrew J. Watson is an academic researcher from University of Exeter. The author has contributed to research in topics: Blastocyst & Embryonic stem cell. The author has an hindex of 88, co-authored 497 publications receiving 34512 citations. Previous affiliations of Andrew J. Watson include Mansfield University of Pennsylvania & Plymouth Marine Laboratory.
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Roles of Na,K-ATPase in early development and trophectoderm differentiation.
TL;DR: The preimplantation embryo offers a unique model for understanding the roles of Na,K-ATPase subunit isoforms in epithelial development and transepithelial transport.
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Physical evolution of the IronEx-I open ocean tracer patch
TL;DR: An 8×8 km tracer-enriched patch was successfully formed in an open-ocean mixed layer in the equatorial Pacific during the first uncontained test of the iron hypothesis as mentioned in this paper.
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Anthropogenic carbon accumulation in the subtropical North Atlantic
TL;DR: In this paper, the authors used a back-calculation shortcut technique and extended multiple linear regression to investigate the accumulation of anthropogenic carbon dioxide (ΔCanth) in the subtropical North Atlantic.
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Chlorofluorocarbon‐derived formation rates of the deep and bottom waters of the Weddell Sea
TL;DR: In this article, the spreading and mixing of deep and bottom waters from the Weddell Sea (originating with potential temperature < 0°C) are investigated through analysis of new and historical CFC measurements.
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Intermediate water from the Greenland Sea in the Faroe Bank Channel : spreading of released sulphur hexafluoride
K. Anders Olsson,Emil Jeansson,Leif G. Anderson,Bogi Hansen,Tor Eldevik,Tor Eldevik,Regin Kristiansen,Marie-José Messias,Truls Johannessen,Truls Johannessen,Andrew J. Watson +10 more
TL;DR: The contribution of the Greenland-Scotland Overflow by intermediate water from the Greenland Sea is investigated by the tracer sulphur hexafluoride (SF6) that was released into the central Greenland Sea in summer 1996 and continuous monitoring has since traced it around the Nordic Seas and into the connecting areas as discussed by the authors.